Cloudnet IWC during POLARSTERN cruise PS106 ...

The dataset contains daily nc-files of the Cloudnet ice water content during Polarstern cruise PS106 based on:- 35.5 GHz Cloud radar MIRA.The data is retrieved using the instrument synergystic approach Cloudnet (Illingworth, 2007, doi:10.1175/BAMS-88-6-883).This variable was calculated from the 35.5...

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Bibliographic Details
Main Authors: Griesche, Hannes, Seifert, Patric, Engelmann, Ronny, Radenz, Martin, Bühl, Johannes
Format: Dataset
Language:English
Published: PANGAEA 2019
Subjects:
Cloudnet
IWC
OCEANET-ATMOSPHERE
PASCAL
PS106
Event label
DATE/TIME
File name
File format
File size
Uniform resource locator/link to file
Remote sensing Light detection and ranging, LiDAR
PS106/1
Polarstern
Arctic Amplification AC3
Arctic
Online Access:https://dx.doi.org/10.1594/pangaea.900246
https://doi.pangaea.de/10.1594/PANGAEA.900246
Description
Summary:The dataset contains daily nc-files of the Cloudnet ice water content during Polarstern cruise PS106 based on:- 35.5 GHz Cloud radar MIRA.The data is retrieved using the instrument synergystic approach Cloudnet (Illingworth, 2007, doi:10.1175/BAMS-88-6-883).This variable was calculated from the 35.5-GHz radar reflectivity factor after correction for gaseous attenuation, and temperature taken from a forecast model, using the following empirical formula:log10(iwc[g m-3]) = 0.000242Z[dBZ]T[degC] + 0.0699Z[dBZ] + -0.0186T[degC] + -1.63 (Hogan, 2006, doi:10.1175/JAM2340.1).In this formula Z is taken to be defined such that all frequencies of radar would measure the same Z in Rayleigh scattering ice. However, the radar is more likely to have been calibrated such that all frequencies would measure the same Z in Rayleigh scattering liquid cloud at 0 degrees C. The measured Z is therefore multiplied by|K(liquid,0degC,35GHz)|^2/0.93 = 0.9441before applying this formula.The formula has been used where the ... : Please note: a newer Version is available, see "Replaced by" reference ...

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